Published in J. Environ. Qual. 32:1743-1749 (2003).
© 2003 ASA, CSSA, SSSA
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TECHNICAL REPORTS
Organic Compounds in the Environment
Organic Manure and Urea Effect on Metolachlor Transport through Packed Soil Columns
Neera Singh*
Division of Agricultural Chemicals, Indian Agricultural Research Institute, New Delhi 110 012, India
* Corresponding author (Drneerasingh{at}yahoo.com).
Received for publication October 26, 2002.
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ABSTRACT
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Application of organic manure (OM) amendments and nitrogen fertilizers can affect the sorption and movement of pesticides in soil. This study summarizes the sorption and leaching of metolachlor [2-chloro-N-(2-ethyl-6-methylphenyl)-N-(2-methoxy-1-methylphenyl)acetamide] in soils after cow (Bos taurus) manure (2.5 and 5.0%) and urea (60 and 120 kg N ha-1) amendments in batch and column experiments. Both cow manure and urea applications increased metolachlor sorption in soils. The values of the Freundlich adsorption parameter Kf(1/n) for treatments T0, T1 (OM), and T2 (OM) were 2.31, 3.32, and 3.96 in Soil 1; 2.02, 2.77, and 3.32 in Soil 2; and 1.10, 1.46, and 2.02 in Soil 3, respectively. Similarly, Kf(1/n) values for treatment T1 (urea) and T2 (urea) were 2.37 and 2.84 in Soil 1; 2.16 and 2.83 in Soil 2; and 1.50 and 1.70 in Soil 3, respectively. Column leaching studies using Soil 1 indicated that OM application drastically reduced the metolachlor leaching losses from 50% (natural soil) to <1.0% (5.0% OM amendment). Likewise, urea application also decreased metolachlor mobility and leaching losses in columns treated with 60 and 120 kg N ha-1 urea were 33 and 20%, respectively. The reduction in the metolachlor leaching losses was achieved through the increase in the sorption capability of the OM- and urea-amended soil. Therefore, coapplication of metolachlor with cow manure or urea fertilizers will not enhance metolachlor mobility and reduces metolachlor leaching losses in low-organic-matter soil.
Abbreviations: DOC, dissolved organic carbon OC, organic carbon OM, organic manure
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INTRODUCTION
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METOLACHLOR IS A SELECTIVE HERBICIDE used for premergence control of annual grasses and broadleaf weeds. Contamination of water resources by pesticide usage has caused public awareness about the quality of drinking water and pollution potential. Water resources may become contaminated by the downward movement (leaching) and runoff (lateral) of soil-applied pesticides. Recent studies addressing the monitoring of pesticides in surface and subsurface water have demonstrated the presence of metolachlor residue (Goodrich et al., 1991; Koterba et al., 1993; Funari et al., 1995; Gaynor et al., 1995; Traub-Eberhard et al., 1995; Sensemann et al., 1997). Peak metolachlor concentration in subsurface drain water discharge of experimental plots ranged from 0.1 mg L-1 (Traub-Eberhard et al., 1995) to more than 100 mg L-1 (Gaynor et al., 1995). The USEPA health advisory level of metolachlor for drinking water is 10 µg L-1.
To assess metolachlor transport to ground water, it is necessary to identify factors involved in the transport. Previous studies have shown that metolachlor transport is influenced by climatic factors, such as timing of rainfall after application (Southwick et al., 1990) and total volume and rate of water application (Sanchez-Martin et al., 1995), and soil properties such as physical structure (Novak et al., 2001) and clay and organic carbon (OC) content. However, among various soil properties, OC content is the single largest factor that has maximum influence on metolachlor adsorption and mobility in soil (Wood et al., 1987; Kruger et al., 1996, Wang et al., 1999, Singh et al., 2002). Thus, metolachlor is susceptible to leaching losses when applied to a coarse-textured soil with low OC content. Therefore, application of OM to low-sorptivity soils can be a promising method to reduce pesticide leaching.
Application of organic carbon in the form of manure, sludge, or crop residues is a common soil management practice followed in agriculture. Generally, addition of OM increases the adsorption of pesticides and decreases their subsequent mobility in the soil profile (Dao, 1991; Guo et al., 1993; Arienzo et al., 1994; Sanchez-Camazano et al., 1997; Cox et al., 1997). Guo et al. (1991)( 1993) studied the sorption of alachlor and atrazine on soils, freshly amended with carbon-rich waste material, and found that the adsorption coefficient for the herbicides was higher in amended soils compared with unamended soils. These results were further confirmed by Barriuso et al. (1997) for eight pesticides in freshly amended soils and Sluszny et al. (1999) in freshly amended and incubated soils. However, there are several instances when application of organic carbon amendments (sewage sludge or compost) resulted in the increased mobility of pesticides, such as atrazine, terbuthylazine, bromacil, or carbofuran (Graber et al., 1995, 2001; Worrell et al., 2001), due to increase in dissolved organic carbon (DOC) content in the soil solution, which complexes with the pesticides and serves as a vehicle for the transport of pesticides to lower soil layers.
Another agronomic practice that can affect the mobility of pesticide through soil layers is the application of nitrogen fertilizers. Liu et al. (1995a)(b) reported that addition of ammonia fertilizers increased the soil pH and DOC concentration resulting in a decrease in atrazine adsorption and an increase in desorption. This led to greater leaching of atrazine through undisturbed soil columns.
The objective of this study was to investigate the effect of cow manure and urea application, common agronomic practices, on metolachlor adsorption and its mobility through packed columns.
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MATERIALS AND METHODS
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Soils
The soils used in the present study were collected from the experimental farms of the Indian Agricultural Research Institute, New Delhi (Soil 1), Pantnagar (Soil 2), and Punjab Agricultural University, Ludhiana (Soil 3). The soil samples were collected from the 0- to 15-cm soil profile, air-dried, and ground to pass through a 2-mm sieve. Before the study, soil samples were stored in plastic bags at room temperature. Physicochemical characteristics of the soils, which were determined using standard methods, are represented in Table 1. Soil pH was determined in a 1:1.25 soil to water suspension using a glass electrode (Jackson, 1967), organic carbon content by the WalkleyBlack method (Walkley and Black, 1934), and soil mechanical fractions by the hydrometer method (Black et al., 1982). The original soil was referred as T0. The cow manure was locally purchased. The physicochemical characteristics of cow manure included a pH of 6.3 and organic carbon of 21.3%. The total carbon, nitrogen, and hydrogen contents of the manure were determined by elemental analysis and were 25.3, 6.7, and 5.8%, respectively.
Chemical
Metolachlor (97.8% purity) was purchased from Riedel de Haen Laborchemikalien GmbH & Co. KG, Seelze, Germany.
Adsorption Experiment
The organic carbon amendment using the cow manure was performed by thoroughly mixing the original soils with air-dried cow manure at 2.5 and 5.0% levels. The manure-amended soils were passed through a 2-mm sieve to ensure thorough mixing of soil and manure. The samples of the amended soil so obtained were labeled as T1 (OM) and T2 (OM), respectively.
Experimental data on sorption in unamended and OM-amended soils was obtained as follows: 5 g of the soil samples [T0, T1 (OM), and T2 (OM)] and 25 mL aqueous solution of metolachlor in 50-mL glass stoppered centrifuge tubes were equilibrated on an end-over-end shaker for 2 h. The kinetics of metolachlor sorption clearly indicated that equilibrium was attained after 2 h of shaking (results not shown). The initial metolachlor concentration ranged between 2 and 20 mg L-1. Four different metolachlor concentrations were used and each concentration was replicated three times. After equilibration, the soilwater suspension was centrifuged at 1500 rpm for 15 min and metolachlor concentration was determined in the supernatant. The amount of metolachlor sorbed was calculated from the difference between the initial and final solution concentrations. Mass balance calculation of metolachlor indicated that metolachlor was stable in the soil during 2 h of equilibration.
To study the effect of urea application on metolachlor sorption, 5-g soil samples in 50-mL glass stoppered centrifuge tubes were mixed with 10 mL aqueous solution of urea. The urea was applied at rates of 60 and 120 kg N ha-1 and treatments were labeled as T1 (urea) and T2 (urea), respectively. Unamended original soils (T0) were supplemented with 10 mL distilled water and served as control. Further, samples T0, T1 (urea), and T2 (urea) were supplemented with 15 mL aqueous solution of metolachlor so that the final metolachlor concentration in all three treatments ranged between 2 and 20 mg L-1. Sorption was studied in a similar manner as mentioned above. The effect of cow manure and urea applications on soil pH and DOC content (Kalembasa and Jenkinson, 1973) was also measured.
Column Experiment
Columns (30-cm length x 6-cm i.d.) were constructed from polyvinyl chloride (PVC) pipe. The PVC columns rested in Buchner funnels fitted with a 0.60-µm nylon membrane to reduce the dead end volume. Only Soil 1 was used for the column experiment. The natural (T0) and cow manureamended soils [T1 (OM) and T2 (OM)] were added to the columns in small increments (approximately 50 g) and after each addition the soil was compacted with equal force to obtain a column of uniform compactness. The columns were packed to bulk densities of 1.46, 1.40, and 1.36 kg L-1, respectively. The pore volume for each column type was calculated from the difference of mass of the soil in a fully saturated column and oven-dry mass of the soil. The values so obtained were 360, 365, and 370 mL for samples T0, T1 (OM), and T2 (OM), respectively. One day before chemical application the columns were pretreated with 500 mL of distilled water to minimize the variation in soil water content between the columns. Water was allowed to drain naturally. Metolachlor (1.875 mg) was applied to the column surface in 2.5 mL acetone in a drop-wise manner and an even metolachlor distribution was assured. This treatment of metolachlor was equivalent to an application rate of 3.8 kg ha-1 (approximately double of normal dose). After herbicide application, the columns were left overnight.
Columns for the urea experiment using natural soil were constructed in a manner as explained above. The columns were packed to a bulk density of 1.46 kg L-1 and the pore water content was 360 mL and was same for untreated and urea-treated columns. Columns were saturated with 500 mL distilled water. Urea treatments were 0, 0.6, and 1.2 mg N cm-2. These doses of urea were equivalent to the field application rates of 60 and 120 kg N ha-1. A 2.5-mL aliquot of water containing 35 or 70 mg of urea was applied drop-wise on the column surface and these treatments were called T1 (urea) and T2 (urea), respectively. The untreated control was labeled T0. Following the urea treatment, metolachlor (1.875 mg) was applied.
Before leaching, the column surfaces were covered with a 0.5-cm DOC-free sand layer to minimize the disturbance of soil and to provide an even distribution of leaching water. One day after herbicide application columns were leached with 1000 mL of distilled water. The water was applied on the column surface at a rate of 100 mL h-1 and natural drainage was allowed. The application rate allowed a water head of approximately 1 cm on the soil surface throughout the leaching. The leachate fractions were collected in approximately 50-mL portions and were analyzed for the metolachlor concentration. Leachate pH and DOC content were also determined. Each column type was replicated twice.
Herbicide Extraction and Analysis
After leaching, soil columns were dissected into 5-cm increments. Each soil section was allowed to air-dry for 48 h. The air-dry samples were transferred to 500-mL stoppered conical flasks and 200 mL hexane was added. The samples were equilibrated on a rotary shaker for 2 h and 50 g of anhydrous Na2SO4 was added to each flask. Metolachlor was quantified by gas chromatography (GC) on a Hewlett-Packard (Palo Alto, CA) Model 3480 equipped with a 63Ni electron capture detector (ECD) and fitted with an HP-1 column (10-m length x 0.50-mm i.d. x 2.53-µm film thickness). The operating conditions were: column, 175°C; injector, 300°C; detector, 300°C; carrier gas (nitrogen) flow rate, 45 mL min-1. The detection limit for metolachlor was 0.1 µg. Metolachlor recovery from soil was more than 80%.
Metolachlor residues from the water samples were extracted by shaking a 5-mL sample with 5 mL hexane for 1 min. After shaking, the sample was allowed to stand for 1 min and 1 g of anhydrous Na2SO4 was added to each tube to remove any trace of moisture from the hexane fraction. Metolachlor residues in the hexane fraction were quantified using GC as mentioned above. Metolachlor recovery from water samples was more than 90%.
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RESULTS AND DISCUSSION
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Adsorption Experiment
Adsorption isotherms for metolachlor in soils are shown in Fig. 1 . The adsorption data were fitted to the Freundlich adsorption equation:
where X is the amount of metolachlor adsorbed (mg kg-1 soil), C is the equilibrium concentration of metolachlor (mg L-1), and Kf and 1/n are the constants. The Freundlich constant Kf represents the amount of metolachlor adsorbed at an equilibrium concentration of 1 mg L-1. The constant 1/n is the measure of the intensity of sorption and reflects the degree to which sorption is the function of herbicide concentration. The values of constants Kf and 1/n are presented in Table 2. The values of the correlation coefficient in all the cases were very high (r2 > 0.953), indicating that the Freundlich adsorption equation satisfactorily explained the results of metolachlor sorption in natural and cow manure or urea-amended soils and were significant at 99% level.
These results clearly indicate that addition of OM increased metolachlor sorption in soils. As both Kf and 1/n are important coefficients for description of adsorption isotherms, especially in case of nonlinear isotherms, Kf(1/n) was selected as a parameter of adsorption. The respective Kf(1/n) values for metolachlor for treatments T0, T1 (OM), and T2 (OM) were 2.31, 3.32, and 3.96 in Soil 1; 2.02, 2.77, and 3.32 in Soil 2; and 1.10, 1.46, and 2.02 in Soil 3. The increased metolachlor sorption in OM-amended soils is positively correlated with the increasing OC content of the cow manureamended soils. The respective OC values for treatments T1 (OM) and T2 (OM) were 1.04 and 2.04% in Soil 1, 1.49 and 3.11% in Soil 2, and 0.95 and 2.02% in Soil 3. Cow manure application decreased soil pH and increased DOC content of the soil (Table 3). Even after a significant increase in DOC content of the soil solution in cow manureamended soils, metolachlor sorption significantly increased. This indicates that metolachlor was sorbed in the bulk-phase organic matter and did not bind to the soluble organic matter. The Kd (partition coefficient) values, calculated from the equation X = KdC, were similar to the Kf values and increased with increasing OC content of the soil.
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Table 3. Influence of cow manure and urea application on soil pH and dissolved organic carbon (DOC) content of soil during sorption experiment.
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Application of urea to the soils also affected metolachlor sorption. The Kf(1/n) values for metolachlor sorption for treatments T0, T1 (urea), and T2 (urea) were 2.31, 2.37, and 2.84 in Soil 1; 2.02, 2.16, and 2.83 in Soil 2; and 1.10, 1.50, and 1.70 in Soil 3, respectively. Therefore, urea application at rates of 60 and 120 kg N ha-1 increased the sorption of metolachlor, a neutral herbicide. Urea application at these rates did not change soil pH and DOC content of the soil solutions during the 2-h equilibration period (Table 3). De Coninck (1980) showed that chemically reactive organic matter of the soil could be influenced by the ionic composition of the soil solution. Similarly, Ghosh and Schnitzer (1980) and Schnitzer (1986) proposed that various soil organic matter components are capable of configurational changes between linear and spherocolloidal shapes and these transformations are dependent on the ionic nature of the solution. Probably, urea application to the soil used in this study has either exposed some of the active sites of the soil organic matter or affected the clay structure, which ultimately resulted in higher metolachlor sorption in the urea-treated soils.
Column Experiment
Figure 2
shows the percolation (breakthrough and cumulative) curves of metolachlor in natural (T0) and cow manureamended [T1 (OM) and T2 (OM)] columns of Soil 1. The results indicate that addition of OM at 2.5 and 5.0% levels drastically reduced the metolachlor movement in packed soil columns. Organic manure application affected both breakthrough time and peak maxima concentration of metolachlor from the soil column. In natural soil columns (T0) metolachlor breakthrough occurred after passing 1.53 pore volumes of water and maximum concentration of metolachlor was obtained after percolating 1.86 pore volumes of water. However, adding 2.5% cow manure to the soil significantly reduced the downward mobility of metolachlor and its breakthrough occurred in the fraction obtained after passing 2.02 pore volumes of water. The metolachlor peak maximum concentration was also reduced by nearly 50%. Likewise, a further increase in cow manure addition to 5.0% [T2 (OM)] further slowed metolachlor movement and its breakthrough occurred after passing 2.36 pore volumes. There was no significant difference in the total amount of leachate collected from the natural and cow manuretreated soil columns (Table 4). However, cow manure application reduced the pH of leachate collected from T1 (OM) and T2 (OM) columns by 0.2 and 0.3 units, respectively. Also, compared with the natural soil column, DOC content of the leachate was 2.7 and 4.8 times higher for T1 (OM) and T2 (OM) columns, respectively, than for the natural soil column (T0). Even after an increase in DOC of the leachate, metolachlor movement was slow in cow manureamended columns. This further proves that metolachlor was bound to bulk-phase organic matter. The decrease in metolachlor movement in organic matteramended soils is in agreement with the results of the batch experiment.

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Fig. 2. (a) Breakthrough and (b) cumulative elution curves of metolachlor in unamended and cow manureamended soil columns. The term C is the amount of metolachlor in the leachate fraction while C0 is the amount applied to the column.
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Figure 3
represents the elution curves of metolachlor in natural (T0) and urea-amended [T1 (urea) and T2 (urea)] columns of Soil 1. Like the cow manure amendment, application of urea to the columns decreased the metolachlor leaching losses and was reflected in its breakthrough time in the leachate. Application of urea at 60 kg N ha-1 rate increased metolachlor breakthrough volume from 1.53 pore volumes (T0) to 2.03 pore volumes [T1 (urea)]. Metolachlor peak maximum was obtained after passing 2.7 pore volumes of water and peak maximum concentration was reduced by 21%. Similar results were obtained at higher urea application of 120 kg N ha-1 and leaching losses of metolachlor were further reduced. There was a slight increase in the pH of leachate collected from the urea-treated columns (Table 4), but DOC increased marginally. The observed increase in the pH of leachate is probably due to the hydrolysis of urea to ammonia. In a separate study the pH of soils treated with urea at 60 and 120 kg N ha-1 doses initially increased by 0.1 and 0.2 units, respectively, was maximum after 48 h of application, and subsequently decreased to original values.

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Fig. 3. (a) Breakthrough and (b) cumulative elution curves of metolachlor in unamended and urea-amended soil columns. The term C is the amount of metolachlor in the leachate fraction while C0 is the amount applied to the column.
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Mass balance calculation of metolachlor from the soil columns (Table 5) indicated that for the natural soil column (T0), nearly 50% of the initially applied metolachlor was recovered from the leachate, while the metolachlor amounts leached out of the T1 (OM) and T2 (OM) columns were 14 and <1.0%, respectively. This study indicates that manure application significantly reduced metolachlor leaching. Thus, the agronomic practice of OM application, usually followed to increase soil fertility, is quite effective in reducing metolachlor leaching . This type of treatment in the northern region of India, where soils are sandy and low in organic matter content, is a useful practice. These results agree with the earlier observations with other chemicals. Guo et al. (1993) studied the movement of alachlor in soils modified by carbon-rich wastes such as waste-activated carbon (WAC), dried municipal waste (DMS), and animal manure (AM). The amount of alachlor recovered from leachate depended on the carbon loading rate of the waste and the source of carbon-containing species, which varied from <0.1% (1.9 Mg [2.1 U.S. tons] C ha-1 of WAC-amended soil) to 74% (unamended soil). Similarly, leaching losses of diuron (Gonzalez-Pradas et al., 1998) and atrazine and MCPA (Socias-Viciana et al., 1999) were drastically reduced in peat-amended soils from Spain.
Application of urea also reduced metolachlor leaching losses (Table 5). At the 60 kg N ha-1 application rate of urea [T1 (urea)], only 33% of the initially applied metolachlor was recovered from the leachate compared with 50% loss of metolachlor from the untreated column. Increasing the urea application rate to 120 kg N ha-1 further decreased the leaching losses and only 10.8% of the metolachlor was recovered in the leachate. This study clearly indicates that coapplication of metolachlor and urea N fertilization in a sandy loam soil significantly reduces the downward movement of metolachlor and that coapplication is a safer practice. These results are well-explained by the greater metolachlor sorption in urea-treated soils than in untreated natural soil.
After leaching of the columns, they were dissected in 5-cm sections and the amounts of metolachlor left in soil after leaching were estimated. Metolachlor distribution in cow manure and urea-amended columns was quite different from the natural soil columns (Fig. 4)
. Metolachlor leached up to a 30-cm depth in both unamended and cow manure or urea-amended soil columns and the amount of metolachlor recovered from the top soil layer (010 cm) was nearly the same in all column types. However, greater amounts of herbicide were retained in the lower soil layers in the cow manure and urea-amended columns compared with the unamended columns. Also, metolachlor movement was not affected by the increase in the DOC content of the cow manureamended soil columns. This study indicates that cow manure and urea amendments may not enhance metolachlor leaching and indeed significantly reduced the leaching losses of herbicide. The inverse relationship between the sorption parameter Kf(1/n) and the percentage of metolachlor recovered from the unamended and cow manure or urea-amended columns suggests that sorption is the key process controlling the movement of metolachlor; however, in field situations biological degradative forces play an important role.
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CONCLUSIONS
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Both cow manure and urea fertilizer amendments increased metolachlor sorption in soils and these amendments also effectively reduced metolachlor leaching losses. The reduction in leaching losses was achieved through increased sorption capability of the amended soils. Therefore, coapplication of organic manureurea and metolachlor is a safe practice as far as metolachlor leaching is concerned. Moreover, these agronomic practices are effective in restricting metolachlor movement. However, due to nonequilibrium physical transport effects and other equilibrium sorption effects, pesticide transport in field trials should be studied.
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